Detecting and Evaluating Hydrodynamic Sealing by Faults
Alton Brown1 and Quentin Fisher2
1 Consultant, Richardson, TX
2 Rock Deformation Research Limited, Leeds, United Kingdom
Hydrodynamic sealing may cause
petroleum
-water contact (PWC) variations across minor faults that do not significantly compartmentalize
reservoir
production. Fault hydrodynamic sealing is analyzed as an extension of classical hydrodynamic sealing theory. Hydrodynamically-sealed faults show two identifying characteristics: (1) water pressure difference across the fault (after correction for the weight of the water), and (2) tilted
petroleum
-water contacts. Maximum height of pure hydrodynamically sealed
petroleum
columns can be predicted from the cross-fault pressure difference. If the
petroleum
accumulation extends across the barrier, the pressures form a single pressure-depth trend, but the PWC will have different elevations. If
petroleum
pressures on different sides of the barrier fall on different trends, then another mechanism must be active in addition to hydrodynamic sealing, such as membrane sealing or hydraulic-resistance sealing. The relative contribution of hydrodynamic sealing can be interpreted from pressure differences, PWC differences, and filling history. These data also help distinguish membrane sealing from hydraulic-resistance sealing.
The potentiometric gradient in hydrodynamically trapped accumulations is calculated from the PWC dip and
fluid
densities. Hydrologically averaged permeability is interpreted from the cross-fault pressure change,
reservoir
potentiometric gradient, and assumed fault width. The membrane-sealing capacity of the fault is estimated from average permeability using empirical trends.
In four field examples, the theoretical relations successfully predicted
properties
of the accumulation or the barrier. In some cases, hydrodynamic theory guided recognition of tilted
fluid
contacts that were previously unrecognized. These case studies substantiate the importance of hydrodynamic sealing by faults in hydrodynamic regimes.